'Europe at the Last Ice Age' Based on Initial Data Compilations
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Project of Strategic Interest NEXTDATA
Project of Strategic Interest NEXTDATA WP 1.2 - GAW-WMO climate observatories Deliverable D1.2.5 Report on the upgrade of GAW-WMO stations with Italian management and related to the SHARE project. WP Coordinator: Angela Marinoni CNR-ISAC Partners: CNR-ISAC, URT Ev-K2-CNR 1 Report on upgrade carried out at GAW Global Stations “O. Vittori” at Monte Cimone and Nepal Climate Observatory Pyramid in the Himalayas 1. “O. Vittori” at Monte Cimone (2165 m, Northern Appenines) The upgrades carried out at Monte Cimone station concern aerosol, gases and radiation measurements. In particular the following measurement programs have been upgraded: - Aerosol size distribution from 10 nm to 800 nm has been completely renewed according to GAW/ACTRIS recommendations. - Aerosol scattering coefficient measured since 2007 at 525 nm has been upgraded with measurement in two additional wave lengths: 450 and 700 nm. Moreover, the following measurement programs have been newly started: - The aerosol size distribution from 500 nm to 20 µm based on time of flight was set up in July 2013. - Radiation measurement program (feasibility study). - Continuous nitrogen oxides (NOx), nitric oxide (NO) and nitrogen dioxide (NO2) measurements suitable for remote high-mountain stations (on test at Bologna laboratories). - Continuous of (SO2) sulfur dioxide measurements is on test in Bologna laboratories, ready for installation at CMN station. - Observations of aerosol vertical profiles have been carried out at Mt. Cimone. After a test installation in October 2012, several improvements were carried out in order to guarantee continuous observations also during winter season. I. Aerosol size distribution from 10 nm to 800 nm The number size distribution of atmospheric aerosol particles is a basic, but essential parameter required in calculations of the effects of aerosols on climate, human health, and eco-systems. -
Climate Signals in a Multispecies Tree-Ring Network from Central And
Clim. Past Discuss., doi:10.5194/cp-2017-48, 2017 Manuscript under review for journal Clim. Past Discussion started: 17 March 2017 c Author(s) 2017. CC-BY 3.0 License. 1 Climate signals in a multispecies tree-ring network from central and 2 southern Italy and reconstruction of the late summer temperatures 3 since the early 1700s 4 5 Giovanni Leonelli1, Anna Coppola2, Maria Cristina Salvatore2, Carlo Baroni2,3, Giovanna Battipaglia4,5, 6 Tiziana Gentilesca6, Francesco Ripullone6, Marco Borghetti6, Emanuele Conte7, Roberto Tognetti7, Marco 7 Marchetti7, Fabio Lombardi8, Michele Brunetti9, Maurizio Maugeri9,10, Manuela Pelfini11, Paolo 8 Cherubini12, Antonello Provenzale3, Valter Maggi1,3 9 10 1 Università degli Studi di Milano–Bicocca — Dept. of Earth and Environmental Science 11 2 Università degli Studi di Pisa — Dept. of Earth Science 12 3 Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche, Pisa 13 4 Università della Campania — Dept. DiSTABiF 14 5 University of Montpellier 2 (France) — PALECO EPHE 15 6 Università degli Studi della Basilicata — School of Agricultural, Forestry, Food and Environmental Sciences, Potenza 16 7 Università degli Studi del Molise — Dept. of Bioscience and Territory 17 8 Università Mediterranea di Reggio Calabria — Dept. of Agronomy 18 9 Istituto di Scienze dell’Atmosfera e del Clima, Consiglio Nazionale delle Ricerche, Bologna 19 10 Università degli Studi di Milano — Dept. of Physics 20 11 Università degli Studi di Milano — Dept. of Earth Science 21 12 Swiss Federal Institute for Forest, Snow and Landscape Research WSL (Switzerland) 22 Correspondence to: Giovanni Leonelli ([email protected]) 23 Abstract. A first assessment of the main climatic drivers that modulate the tree-ring width (RW) and maximum latewood 24 density (MXD) along the Italian Peninsula and northeastern Sicily was performed using 27 forest sites, which include conifers 25 (RW and MXD) and broadleaves (only RW). -
Cryogenian Glaciation and the Onset of Carbon-Isotope Decoupling” by N
CORRECTED 21 MAY 2010; SEE LAST PAGE REPORTS 13. J. Helbert, A. Maturilli, N. Mueller, in Venus Eds. (U.S. Geological Society Open-File Report 2005- M. F. Coffin, Eds. (Monograph 100, American Geophysical Geochemistry: Progress, Prospects, and New Missions 1271, Abstracts of the Annual Meeting of Planetary Union, Washington, DC, 1997), pp. 1–28. (Lunar and Planetary Institute, Houston, TX, 2009), abstr. Geologic Mappers, Washington, DC, 2005), pp. 20–21. 44. M. A. Bullock, D. H. Grinspoon, Icarus 150, 19 (2001). 2010. 25. E. R. Stofan, S. E. Smrekar, J. Helbert, P. Martin, 45. R. G. Strom, G. G. Schaber, D. D. Dawson, J. Geophys. 14. J. Helbert, A. Maturilli, Earth Planet. Sci. Lett. 285, 347 N. Mueller, Lunar Planet. Sci. XXXIX, abstr. 1033 Res. 99, 10,899 (1994). (2009). (2009). 46. K. M. Roberts, J. E. Guest, J. W. Head, M. G. Lancaster, 15. Coronae are circular volcano-tectonic features that are 26. B. D. Campbell et al., J. Geophys. Res. 97, 16,249 J. Geophys. Res. 97, 15,991 (1992). unique to Venus and have an average diameter of (1992). 47. C. R. K. Kilburn, in Encyclopedia of Volcanoes, ~250 km (5). They are defined by their circular and often 27. R. J. Phillips, N. R. Izenberg, Geophys. Res. Lett. 22, 1617 H. Sigurdsson, Ed. (Academic Press, San Diego, CA, radial fractures and always produce some form of volcanism. (1995). 2000), pp. 291–306. 16. G. E. McGill, S. J. Steenstrup, C. Barton, P. G. Ford, 28. C. M. Pieters et al., Science 234, 1379 (1986). 48. -
The Last Maximum Ice Extent and Subsequent Deglaciation of the Pyrenees: an Overview of Recent Research
Cuadernos de Investigación Geográfica 2015 Nº 41 (2) pp. 359-387 ISSN 0211-6820 DOI: 10.18172/cig.2708 © Universidad de La Rioja THE LAST MAXIMUM ICE EXTENT AND SUBSEQUENT DEGLACIATION OF THE PYRENEES: AN OVERVIEW OF RECENT RESEARCH M. DELMAS Université de Perpignan-Via Domitia, UMR 7194 CNRS, Histoire Naturelle de l’Homme Préhistorique, 52 avenue Paul Alduy 66860 Perpignan, France. ABSTRACT. This paper reviews data currently available on the glacial fluctuations that occurred in the Pyrenees between the Würmian Maximum Ice Extent (MIE) and the beginning of the Holocene. It puts the studies published since the end of the 19th century in a historical perspective and focuses on how the methods of investigation used by successive generations of authors led them to paleogeographic and chronologic conclusions that for a time were antagonistic and later became complementary. The inventory and mapping of the ice-marginal deposits has allowed several glacial stades to be identified, and the successive ice boundaries to be outlined. Meanwhile, the weathering grade of moraines and glaciofluvial deposits has allowed Würmian glacial deposits to be distinguished from pre-Würmian ones, and has thus allowed the Würmian Maximum Ice Extent (MIE) –i.e. the starting point of the last deglaciation– to be clearly located. During the 1980s, 14C dating of glaciolacustrine sequences began to indirectly document the timing of the glacial stades responsible for the adjacent frontal or lateral moraines. Over the last decade, in situ-produced cosmogenic nuclides (10Be and 36Cl) have been documenting the deglaciation process more directly because the data are obtained from glacial landforms or deposits such as boulders embedded in frontal or lateral moraines, or ice- polished rock surfaces. -
Moüjmtaiim Operations
L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot. -
6.Peaks in 5 Days
6 Peaksin 5 Days Not surprisingly, scaling incredible summits ranks among the most popular activities in the Alps -- including iconic peaks like the Matterhorn, the mystical Wildspitze glacier, or the vertigo-inducing Zugspitze. But if climbing isn’t your thing, you can take a cable car to the tops of these peaceful giants and enjoy the views, sans ice pick. Breathtaking view of the Zugspitze, Germany’s highest peak Germany MUNICH SALZBURG 6 BERCHTESGADEN 4 GARMISCH ZURICH Austria 5 HOHE TAUERN Switzerland 3 ÖTZTAL 2 GSTAAD 1ZERMATT 1Zermatt Picturesque Zermatt lies at the foot of the fabled Matterhorn, one of the world’s iconic mountains. The popular, car-free destination has preserved its original character and offers nearly unlimited possibilities for fun, including skiing, climbing, and hiking, as well as boutique shopping and outdoor ice-skating and curling rinks. STAY EAT DO The Omnia Mountain Lodge At Cervo Mountain Boutique Zermatt cable cars take visitors to claims pride of place on a rock Resort, Alpine-chalet design Europe’s highest mountain station high above Zermatt. merges with a hint of hunting lodge. and the Matterhorn Glacier Paradise. At the Matterhorn’s foot sits the The Cervo-Puro Restaurant boasts Gorner Gorge ranks among the most four-star superior Romantik 14 GaultMillau points. Restaurant breathtaking natural beauties of Hotel Julen, featuring 1818 serves modern Alpine cuisine. Zermatt. spruce-paneled rooms. myswitzerland.com/the-omnia-mountain-lodge myswitzerland.com/hotel-cervo.html myswitzerland.com/zermatt.htm myswitzerland.com/romantik-hotel-julen myswitzerland.com/restaurant-1818 myswitzerland.com/gorner-gorge See Amazing Blacknose Sheep Visit the legendary Blacknose Sheep in the stable of the Julen family every Wednesday. -
Sea Level and Global Ice Volumes from the Last Glacial Maximum to the Holocene
Sea level and global ice volumes from the Last Glacial Maximum to the Holocene Kurt Lambecka,b,1, Hélène Roubya,b, Anthony Purcella, Yiying Sunc, and Malcolm Sambridgea aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; bLaboratoire de Géologie de l’École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and cDepartment of Earth Sciences, University of Hong Kong, Hong Kong, China This contribution is part of the special series of Inaugural Articles by members of the National Academy of Sciences elected in 2009. Contributed by Kurt Lambeck, September 12, 2014 (sent for review July 1, 2014; reviewed by Edouard Bard, Jerry X. Mitrovica, and Peter U. Clark) The major cause of sea-level change during ice ages is the exchange for the Holocene for which the direct measures of past sea level are of water between ice and ocean and the planet’s dynamic response relatively abundant, for example, exhibit differences both in phase to the changing surface load. Inversion of ∼1,000 observations for and in noise characteristics between the two data [compare, for the past 35,000 y from localities far from former ice margins has example, the Holocene parts of oxygen isotope records from the provided new constraints on the fluctuation of ice volume in this Pacific (9) and from two Red Sea cores (10)]. interval. Key results are: (i) a rapid final fall in global sea level of Past sea level is measured with respect to its present position ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y and contains information on both land movement and changes in before present (30 ka BP); (ii) a slow fall to −134 m from 29 to 21 ka ocean volume. -
Chapter 4 Member States of the European Union and The
CHAPTER 4 membeR StAteS oF tHe EuroPean UnioN and tHe EuroPean EcoNomic AReA 4.1 Austria ............................................. 18 4.15 Latvia .............................................. 50 4.2 belgium ........................................... 20 4.16 lithuania ......................................... 52 4.3 Cyprus ............................................. 24 4.17 luxembourg ................................... 55 4.4 Czech Republic ............................... 26 4.18 Malta ............................................... 59 4.5 denmark ......................................... 29 4.19 Netherlands ..................................... 61 4.6 estonia ............................................. 31 4.20 Norway ............................................ 64 4.7 Finland ............................................ 33 4.21 Poland .............................................. 66 4.8 France.............................................. 35 4.22 Portugal ........................................... 69 4.9 Germany ......................................... 37 4.23 Slovakia ........................................... 71 4.10 Greece .............................................. 39 4.24 Slovenia ........................................... 74 4.11 Hungary .......................................... 41 4.25 Spain ................................................ 76 4.12 Iceland ............................................. 43 4.26 Sweden ............................................. 81 4.13 Ireland ............................................ -
Rifugio Campo Imperatore + Center for Ecotourism and Cultural Creativity
CAMPO IMPERATORE Center for Ecotourism + Cultural Creativity ANALYSIS, RESEARCH AND DESIGN FOR THE REQUALIFICATION OF NEGLECTED SPACES Prepared by Elsa G. De Leon ENVIRONMENT LOCATION Parco Nazionale del Gran Sasso e Monti della Laga Provincia di Terramo Urbino Provincia Marche di Pescara Abruzzo Campo L’Aquila Provincia Imperatore Lazio di Chieti Roma Campo Imperatore Parco Nazionale della Parco Nazionale Provincia Majella dell’Aquila d’Abruzzo ABRUZZO - ITALY. Italian Region. PROVINCIA DELL’AQUILA. Abruzzo Province. GRAN SASSO. National Park. CAMPO IMPERATORE. Alpine meadow. ASCOLIPICENO CULTURAL + VALUES SAN GIACOMO L’ecomuseo di Valle Castellana Ripe Valle Castellana Lago di CEPPO Campotosto L’ecomuseo di Lago di Valle Castellana Campotosto TERAMO AMATRICE CAMPOTOSTO PIETRACAMELA ISOLA DEL GRAN SASSO Arsita Prati di Tivo S. Pietro CAMPO IMPERATORE Museo del Camoscio Orto Botanico Appenninico di San Colombo FONTE VETICA FONTE CERRETO Farindola Arischia Assergi LAGO RACOLLO S. Stefano di Sessanio L’AQUILA Barisciano Calascio PARCO NAZIONALE L’Aquila Centro GRAN SASSO E MONTI DELLA LAGA Visite Fiume Tirino Bussi sul Tirino Historic Center km 0 1 2 3 4 5 km ENVIRONMENTAL + CULTURAL VALUES 150.000 3 5 44 HECTARES REGIONS PROVINCES MUNICIPALITIES BIODIVERSITY AGRO-BIODIVERSITY 51 In danger flora Cereals Solina, Farro Rosso 59 Spontaneous Orchids Legumes Lentils of Santo Stefano di Sessanio 2 Carnivorous plants Vegetables Red Potato Aromatic Plants Tansy, Customary 2364 Register Plants Fruit Trees Apples, figs, Mediterranean hack berry, almonds -
4000 M Peaks of the Alps Normal and Classic Routes
rock&ice 3 4000 m Peaks of the Alps Normal and classic routes idea Montagna editoria e alpinismo Rock&Ice l 4000m Peaks of the Alps l Contents CONTENTS FIVE • • 51a Normal Route to Punta Giordani 257 WEISSHORN AND MATTERHORN ALPS 175 • 52a Normal Route to the Vincent Pyramid 259 • Preface 5 12 Aiguille Blanche de Peuterey 101 35 Dent d’Hérens 180 • 52b Punta Giordani-Vincent Pyramid 261 • Introduction 6 • 12 North Face Right 102 • 35a Normal Route 181 Traverse • Geogrpahic location 14 13 Gran Pilier d’Angle 108 • 35b Tiefmatten Ridge (West Ridge) 183 53 Schwarzhorn/Corno Nero 265 • Technical notes 16 • 13 South Face and Peuterey Ridge 109 36 Matterhorn 185 54 Ludwigshöhe 265 14 Mont Blanc de Courmayeur 114 • 36a Hörnli Ridge (Hörnligrat) 186 55 Parrotspitze 265 ONE • MASSIF DES ÉCRINS 23 • 14 Eccles Couloir and Peuterey Ridge 115 • 36b Lion Ridge 192 • 53-55 Traverse of the Three Peaks 266 1 Barre des Écrins 26 15-19 Aiguilles du Diable 117 37 Dent Blanche 198 56 Signalkuppe 269 • 1a Normal Route 27 15 L’Isolée 117 • 37 Normal Route via the Wandflue Ridge 199 57 Zumsteinspitze 269 • 1b Coolidge Couloir 30 16 Pointe Carmen 117 38 Bishorn 202 • 56-57 Normal Route to the Signalkuppe 270 2 Dôme de Neige des Écrins 32 17 Pointe Médiane 117 • 38 Normal Route 203 and the Zumsteinspitze • 2 Normal Route 32 18 Pointe Chaubert 117 39 Weisshorn 206 58 Dufourspitze 274 19 Corne du Diable 117 • 39 Normal Route 207 59 Nordend 274 TWO • GRAN PARADISO MASSIF 35 • 15-19 Aiguilles du Diable Traverse 118 40 Ober Gabelhorn 212 • 58a Normal Route to the Dufourspitze -
The Climate of the Last Glacial Maximum: Results from a Coupled Atmosphere-Ocean General Circulation Model Andrew B
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 104, NO. D20, PAGES 24,509–24,525, OCTOBER 27, 1999 The climate of the Last Glacial Maximum: Results from a coupled atmosphere-ocean general circulation model Andrew B. G. Bush Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada S. George H. Philander Program in Atmospheric and Oceanic Sciences, Department of Geosciences, Princeton University Princeton, New Jersey Abstract. Results from a coupled atmosphere-ocean general circulation model simulation of the Last Glacial Maximum reveal annual mean continental cooling between 4Њ and 7ЊC over tropical landmasses, up to 26Њ of cooling over the Laurentide ice sheet, and a global mean temperature depression of 4.3ЊC. The simulation incorporates glacial ice sheets, glacial land surface, reduced sea level, 21 ka orbital parameters, and decreased atmospheric CO2. Glacial winds, in addition to exhibiting anticyclonic circulations over the ice sheets themselves, show a strong cyclonic circulation over the northwest Atlantic basin, enhanced easterly flow over the tropical Pacific, and enhanced westerly flow over the Indian Ocean. Changes in equatorial winds are congruous with a westward shift in tropical convection, which leaves the western Pacific much drier than today but the Indonesian archipelago much wetter. Global mean specific humidity in the glacial climate is 10% less than today. Stronger Pacific easterlies increase the tilt of the tropical thermocline, increase the speed of the Equatorial Undercurrent, and increase the westward extent of the cold tongue, thereby depressing glacial sea surface temperatures in the western tropical Pacific by ϳ5Њ–6ЊC. 1. Introduction and Broccoli, 1985a, b; Broccoli and Manabe, 1987; Broccoli and Marciniak, 1996]. -
Deglacial Permafrost Carbon Dynamics in MPI-ESM
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-54 Manuscript under review for journal Clim. Past Discussion started: 6 June 2018 c Author(s) 2018. CC BY 4.0 License. Deglacial permafrost carbon dynamics in MPI-ESM Thomas Schneider von Deimling1,2, Thomas Kleinen1, Gustaf Hugelius3, Christian Knoblauch4, Christian Beer5, Victor Brovkin1 1Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg, Germany 2 5 now at Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 14473 Potsdam, Germany 3Department of Physical Geography and Bolin Climate Research Centre, Stockholm University, SE10693, Stockholm, Sweden 4Institute of Soil Science, Universität Hamburg, Allende-Platz 2, 20146 Hamburg, Germany 5Department of Environmetal Science and Analytical Chemistry and Bolin Centre for Climate Research, Stockholm 10 University, 10691 Stockholm, Sweden Correspondence to: Thomas Schneider von Deimling ([email protected]) Abstract We have developed a new module to calculate soil organic carbon (SOC) accumulation in perennially frozen ground in the 15 land surface model JSBACH. Running this offline version of MPI-ESM we have modelled permafrost carbon accumulation and release from the Last Glacial Maximum (LGM) to the Pre-industrial (PI). Our simulated near-surface PI permafrost extent of 16.9 Mio km2 is close to observational evidence. Glacial boundary conditions, especially ice sheet coverage, result in profoundly different spatial patterns of glacial permafrost extent. Deglacial warming leads to large-scale changes in soil temperatures, manifested in permafrost disappearance in southerly regions, and permafrost aggregation in formerly glaciated 20 grid cells. In contrast to the large spatial shift in simulated permafrost occurrence, we infer an only moderate increase of total LGM permafrost area (18.3 Mio km2) – together with pronounced changes in the depth of seasonal thaw.